- WOK 4-47
- Item
- [1948-1957]
Part of W.O. Kupsch fonds
Formation of esker in ice-age. Sand and gravel sedimentation in meltwater tunnel of crevasse in moraine-choked glacier ice or dead-ice. The shape of the esker formed after the melting of the ice by soil slipping from the ice-contact walls. Source: Atlas of Denmark.